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Article: Field structural-lithofacie zones for shear remelt granite of Lianyunshan in Hunan province

TitleField structural-lithofacie zones for shear remelt granite of Lianyunshan in Hunan province
Authors
Li, XLi, JZhou, M
KeywordsDynamic Metamorphism-Shear Remelt Magmatism
Lianyunshan Granite
Nne-Trending Strike-Slip Fault
Issue Date2001
Publisher中國地質大學. The Journal's web site is located at http://dzkq.chinajournal.net.cn/
Citation
Dizhi Keji Qingbao/Geological Science And Technology Information, 2001, v. 20 n. 3, p. 27-30 How to Cite?
AbstractThe lenticular granite of Lianyunshan in Hunan is located in the strike-slip fault zone of Changshoujie-Shuangpai. The field geological survey across the granite, shows that there are continuously transitional structural-lithofacie zones: Lengjiaxi Group (adjacent rock) without fault dynamic metamorphism→mica-quartz tectonic schist bearing garnet→migmatitic quartz-mica schist→banded and ptygmatic migmatite including small rock masses of lenticular granite→gneissic and massive biotite monzonitic granite (host rock). The analyses of regional structures show that Lianyunshan granite is associated with dynamic metamorphism-shear remelt magmatism of NNE-trending convergent strike-slip faulting during T3-J.
Persistent Identifierhttp://hdl.handle.net/10722/151073
ISSN
1000-7849

 

DC FieldValueLanguage
dc.contributor.authorLi, Xen_US
dc.contributor.authorLi, Jen_US
dc.contributor.authorZhou, Men_US
dc.date.accessioned2012-06-26T06:16:47Z-
dc.date.available2012-06-26T06:16:47Z-
dc.date.issued2001en_US
dc.identifier.citationDizhi Keji Qingbao/Geological Science And Technology Information, 2001, v. 20 n. 3, p. 27-30en_US
dc.identifier.issn1000-7849en_US
dc.identifier.urihttp://hdl.handle.net/10722/151073-
dc.description.abstractThe lenticular granite of Lianyunshan in Hunan is located in the strike-slip fault zone of Changshoujie-Shuangpai. The field geological survey across the granite, shows that there are continuously transitional structural-lithofacie zones: Lengjiaxi Group (adjacent rock) without fault dynamic metamorphism→mica-quartz tectonic schist bearing garnet→migmatitic quartz-mica schist→banded and ptygmatic migmatite including small rock masses of lenticular granite→gneissic and massive biotite monzonitic granite (host rock). The analyses of regional structures show that Lianyunshan granite is associated with dynamic metamorphism-shear remelt magmatism of NNE-trending convergent strike-slip faulting during T3-J.en_US
dc.languageengen_US
dc.publisher中國地質大學. The Journal's web site is located at http://dzkq.chinajournal.net.cn/zh_HK
dc.relation.ispartofDizhi Keji Qingbao/Geological Science and Technology Informationen_US
dc.subjectDynamic Metamorphism-Shear Remelt Magmatismen_US
dc.subjectLianyunshan Graniteen_US
dc.subjectNne-Trending Strike-Slip Faulten_US
dc.titleField structural-lithofacie zones for shear remelt granite of Lianyunshan in Hunan provinceen_US
dc.typeArticleen_US
dc.identifier.emailZhou, M:mfzhou@hkucc.hku.hken_US
dc.identifier.authorityZhou, M=rp00844en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0035441228en_US
dc.identifier.volume20en_US
dc.identifier.issue3en_US
dc.identifier.spage27en_US
dc.identifier.epage30en_US
dc.publisher.placeChinaen_US
dc.identifier.scopusauthoridLi, X=8319382400en_US
dc.identifier.scopusauthoridLi, J=27172256800en_US
dc.identifier.scopusauthoridZhou, M=7403506005en_US
dc.identifier.issnl1000-7849-

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